E. Thomas et al., Water adsorption by hydrophobic organic surfaces: Experimental evidence and implications to the atmospheric properties of organic aerosols, J GEO RES-A, 104(D13), 1999, pp. 16053-16059
The adsorption of water on hydrophobic organized organic thin films, used a
s a proxy for atmospheric organic aerosols, was measured simultaneously wit
h a molecularly controlled semiconductor resistor (MOCSER) and quartz cryst
al microbalance (QCM). Water adsorption was found to be reversible and depe
ndent on relative humidity (RH). The MOCSER measurements show that the adso
rption kinetics of the first water layer resembles Langmuir behavior. The Q
CM findings indicate that adsorption is proportional to the water vapor pre
ssure and exceeds the amount equivalent to one monolayer. These results can
be explained by the formation of small water clusters on imperfections or
structural defects on the organic surface and that the water does not achie
ve complete surface coverage even at high relative humidity. This mechanism
resembles previous observations of water adsorption to structural defects
on inorganic crystals. It is also shown that water can penetrate through th
e organic surface and reach the inorganic surface, even with a closely pack
ed organic coating. This paper presents applications of these findings to t
he properties of organic aerosols.